Sunday, March 27, 2011

Science Friday had an entertaining talk with Michael Collins of Texas State University about the discovery of blades and spear points in Texas that pre date Clovis tools which are thought by many to represent the earliest people in the Americas.

From the transcript:

FLATOW: But why do you go deeper, where some other scientists might have stopped?

Dr.
COLLINS: Well, we're working against an inertia, two inertias, really,
that one has said for very many years that Clovis was the oldest culture
in the Americas, at around 13,000 to 13,200 or 13,300 years ago. And
some people haven't gotten over that, in spite of the fact for the last
nearly 20 years we have had quite a few sites with strong indications of
people being here before Clovis

.

And
another thing - and that's improving. More and more people are accepting
the concept or are at least willing to investigate it.

The
other thing, the other inertia that we have, and it's also improving
rapidly and greatly: American archaeology has - grew up in the social
sciences.

And not long ago, the vast
majority of practicing archeologists in this country had very little
background in the earth sciences and consequently didn't really think
about the fact that okay, I have found cultural material here, I'm
backing this excavation to Clovis, so that's the oldest culture, I'll
just quit here, without thinking: You know, the dirt below that is just a
little bit older. Why don't I look at that and see what's in it? There
just wasn't that - that mindset was not particularly common. But
happily, both of those things are changing for the better.

I find the stuff about the lack of earth sciences background hindering exploration a little hard to swallow. You don't need a background in earth sciences to motivate yourself to poke around in slightly older layers.

Just common sense..and perhaps overcoming the first inertia that a mainstream theory could be wrong.

This is a good resource organized in the form of questions and answers on geological evidence for climate change. You will be able to learn a lot about past fluctuations in climate, the establishment of the post-Eocene cooling regime, the Pleistocene ice ages and their causes and the role CO2 has played through geological history, mostly as an amplifier of warming.

The U.K Geological Society also firmly states and although there are natural drivers of climate change, burning of fossil fuels has contributed significantly to the current warming trend.

Wednesday, March 23, 2011

..The scientists discovered that quartz crystal deposits are found
wherever mountains or fault lines occur in states like California,
Idaho, Nevada and Utah.

The Utah State geoscientist said the
breakthrough came after repeated testing revealed a correlation between
quartz deposits and geologic events that was "completely eye-popping."

Using
newly developed remote sensing technology known as Earthscope, Lowry
and Perez-Gussinye found that quartz indicates a weakness in the earth's
crust likely to spawn a geologic event such as an earthquake or a
volcano.

In this post-Japan atmosphere of heightened awareness, hype, hyperbole and sensational claims about earthquakes and volcanoes it is important to set the geology straight.

The paper is behind a paywall and I have not read it, but from the abstract I could gather -

The study addresses variations in the presence of crustal quartz and whether it may influence localization of continental scale deformation due to quartz being weaker than other minerals. The study is on the continental scale and when geologists speak of crustal quartz they mean the mineral that makes up part of the bulk of the rock. Crust with high amounts of quartz would mean crust made up of rocks like granites, granite gneisses and quartz rich schists and quartzites. So variations in the bulk composition of the crust over hundreds of kilometers may influence where deformation occurs and persists over geological time.

Tuzo Wilson imagined the crust being recycled by the repeated opening (rifting) and closing (collisions) of continents, the famous Wilson cycle. This study suggests that such opening of continents may be initiated in quartz rich zones of the crust and these previously rifted and weakened zones are then more likely to break into rifts or deform into mountain belts during subsequent tectonic events thus localizing deformation over many cycles.

The press release though mutates crustal quartz into crystal quartz deposits accompanied by a picture of an amethyst crystal cluster and announces that such crystal quartz deposits may help us predict earthquakes. Crystal quartz deposits and crustal quartz mean different things to geologists. Crustal quartz as I explained above refers to the mineral quartz that is pervasive throughout the crust making up a proportion of the rock mass along with other minerals.

On the other hand the term crystal quartz deposits usually is taken to mean veins cutting across the rock mass or cavities in the rock which are filled with quartz crystals often as pretty faceted forms. These may occur over very small regions of a few hundred meters to a few kilometers or so and sometimes quartz may occur in concentrations that can be mined.

These types of small segregated deposits of quartz do not automatically indicate an increased likelihood of earthquakes in that particular area. At the most they may point to the presence of a fault. For example fault zones contain fractured rock. Mineralizing fluids containing silica may precipitate quartz concentrations along these fractures. However geologists don't make a leap and announce that an earthquake is likely along that fault anytime in the future based on the presence of these crystal quartz deposits.

Quartz deposits by themselves don't tell us anything about the stress levels the crust is under and whether the fault may slip anytime soon. Independent monitoring of stress levels along faults using sensitive instruments is just beginning to be used in some areas but we are a long way away from using that information to make predictions about an earthquake.

Coming back to the paper...Large continental zones over which the crust has been deformed such as rifts, collision zones or subduction zones are also regions where earthquakes are more likely to occur. We already know that. But while there may be a correlation between crustal quartz amount and such large zones of deformation, that does not translate into specific predictions about where and when earthquakes may occur in these zones. The study certainly does not claim any such advance in our understanding of earthquakes.

I had a thought though about the correlation between quartz rich crustal zones and repeated deformation. Think about the early Archean when continents were forming. What would be the future Indian continent is a collage of several such continental nuclei which welded to each other over the Archean and early Proterozoic. An example is the zone of continental deformation along the Narmada rift in central India which has seen suturing and rifting of continental blocks repeatedly in the Archean and early-mid Proterozoic.

The first location of collision between continental nuclei was not controlled by the presence of quartz but was just happenstance. That initial collision, the zone of suture along which the two continents stuck to each other became the prime zone of weakness in the larger continental block. And during collision that zone likely became richer in quartz as partial melting of the old crust formed differentiated quartz-rich new crust.

This crust because it was weak from a previous collision/deformation event was reactivated during subsequent tectonic events and became even richer in quartz following repeated magmatic and sedimentary differentiation of the crust during each such event.

Is there really a quartz enrichment trend in the Precambrian crust of the Narmada rift? Is quartz rich crust the cause or the consequence of localized crustal deformation? Maybe the relation is different in different settings..maybe there are feedbacks...

Tuesday, March 22, 2011

Sam Roberts in the New York Times writes on the 200th birthday for the certification by city commissioners of a map by John Randel which subdivided Manhattan island into a two dimensional street grid with rectangular plots on which modern Manhattan arose.

The grid was the great leveler. By shifting millions of cubic yards of
earth and rock, it carved out modest but equal flat lots (mostly 25 by
100 feet) available for purchase. And if it fostered what de Tocqueville
viewed as relentless monotony, its coordinates also enabled drivers and
pedestrians to figure out where they stood, physically and
metaphorically.

“This is the purpose of New York’s geometry,” wrote Roland Barthes, the
20th-century French philosopher. “That each individual should be
poetically the owner of the capital of the world.”

Thursday, March 17, 2011

The Atlantic is in most places not at all like the Pacific or the Indian oceans - it is not dominated by the color blue, nor is it overwhelmingly fringed with leaning palm trees and coral reefs. It is a grey and heaving sea, not infrequently storm-bound, ponderous with swells, a sea that in the mind's eye is thick with trawlers lurching, bows up, then crashing down through great white curtains of spume, tankers wallowing though the swells, its weather so often on the verge of gales, and all the while its waters moving with an air of settled purpose, simultaneously displaying incalculable power, and inspiring by this display perpetual admiration, respect, caution and fear.

The Atlantic is the classic ocean of our imaginings, an industrial ocean of cold and iron and salt, a purposeful ocean of sea-lanes and docksides and fisheries, an ocean alive with squadrons of steadily moving ships above, with unimaginable volumes of mysterious marine abundance below. It is also an entity that seems to be somehow interminable. Year in and year out, night and day, warm and cold, century after century, the ocean is always there, an eternal presence in the collective minds of those who live beside it.

As with many of his other books there is a lot of geology in this one too, but it is evocative passages like these that I enjoy the most.

Tuesday, March 15, 2011

New York Times carried a story on the controversial resignation of German Defence Minister Mr. Guttenburg on allegations that he plagiarized parts of his doctoral thesis.

On what a degree means in Germany:

Ms. Merkel, a former academic married to a professor, was being accused
of belittling intellectual property theft and, by implication, the value
of an advanced degree, which is not a purely academic matter in this
country. Many jobs require such degrees in Germany, where, as is not the
case in America, calling oneself doctor for having completed a thesis
in, say, political science or art history, is not embarrassing but
normal, even when filling out Lufthansa’s online booking forms. (The
airline generously provides three levels of academic achievement for its
overachieving countrymen: doctor, professor and professor doctor,
skipping the extremely rare but not unheard-of German mouthful Herr
Professor Doctor Doctor).

If I had to fill a Lufthansa online booking form I would be the lowest rung...just a .. Doctor.

Friday, March 11, 2011

From a note in Geospatial World I learn that the Election Commission (EC) of India might be using Google satellite images as a background layer on which to placemark the locations of polling booths along with relevant information. The project will be initiated in the state of Bengal.

If this report of using Google is true, I am curious to know why the EC chose Google over Bhuvan which also serves out satellite images and is advertised by the Indian Space Research Organization (ISRO) to be customizable to incorporate the kind of functionality the EC wants.

Is it because - a) the EC was not aware of Bhuvan and its capabilities? In that case, ISRO has not done a good job of educating potential users about Bhuvan.

Or is it because - b) the Application Programming Interface i.e. the programming tools that allow developers to customize the application is not good enough?

Or is it because - c) Data policy restricts even government departments from accessing very high resolution imagery (1 meter) from Indian satellites for web applications, even internal ones like the proposed polling booth app. Government users may obtain without clearances high res images of a pre-defined extent i.e. images of one particular geographic area, but is a high res seamless image stream available to them through Bhuvan?

Currently the data policy allows only imagery of resolution 5.8 meters and coarser to be released free of clearances in the public domain. Due to this policy Bhuvan can only stream images of 5.8 meters and coarser to the general public. The policy is supposed to be up for a review this year.

Whatever the reasons, it's a shame that Bhuvan and high resolution imagery captured by Indian satellites is being kept away from being utilized in innovative applications.

Saturday, March 5, 2011

I've written before ( 123) on hydrogeologically complex aquifers of Deccan Basalts and other hard rock terrains in India and how they influence farmer livelihoods by controlling access to groundwater.

Mysaiah et al have published a paper (open access) in Current Science on the use of ground penetrating radar in imaging subsurface fracture systems (sheet joints) in granitic terrains around the city of Hyderabad.They suggest in their paper that this sort of information will be useful for modeling and understanding groundwater flow in shallow aquifers as well as a host of other engineering applications.

I wonder if this technique can be adapted by state groundwater agencies to survey large tracts of land when mapping aquifer potential in other hard rock terrains like Deccan Basalts. This volcanic terrain too has a rock structure interrupted by horizontal sheet joints which control storage and flow of groundwater. The image below of a dug well shows ground water flowing out of the sheet joint in basalts.

State agencies when compiling working plans usually use the local watershed as the hydrologic unit when delineating aquifers. This in the end translates into a sort of generalized advice on groundwater potential and management to farmers. This is often of little use to especially small land owners who are farming plots less than a couple of acres or so. This scale of mapping will say nothing about what lies beneath such small plots.

Yet it is these small land owners who are in the most need of very specific advice on groundwater potential. In large regions of the Deccan Basalts and also in the granitic terrains of south India, monsoons and groundwater are the only source of water.

Farmers livelihoods depends on the aquifer properties. For making informed decisions on investing on drilling or digging for water, farmers would like to know whether fracture systems that could potentially yield water underlie their fields or whether they are sitting on top of a likely unyielding basalt or granite monolith. These are the types of investments which if they fail result in the farmer going down a path of indebtedness from which it is not easy for them to recover.

At a community level too there are movements now in India for farmers to form village level water sharing cooperatives and such surveys may lead to better ground water management practices.

Land based radar surveys of large areas may be cumbersome and
expensive.. but it is an investment in technology and basic data generation
that the government should give serious thought to - for it will result in a detailed and more site specific understanding of the shallow ground water system on which millions of farmers in India rely upon.

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ABOUT THIS BLOG

I am a Sedimentary Geologist. On Rapid Uplift I write mostly about topics within the geosciences, but sometimes on biological evolution and environmental issues. I like to travel and in my free time I teach 12 year old kids soccer and rugby.